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本文用电子顺磁共振方法详细地分析了贵州省晴隆大厂锑矿田各种矿物锰离子的存在形式,并结合众多的化学分析资料,阐述了矿田中锰离子的分配规律及与锑矿化的关系,指出在大厂矿田的成岩成矿过程中,锰没有象锑那样充分转移富集,其地球化学行为表现为一种“惰性”,各类矿物和岩石中锰的含量均很低,没有锰的载体矿物形成。同时,还进一步论述了对锰离子的研究在解决金属矿床某些问题时具有成因方面和找矿方面的双重意义。
In this paper, the electronic paramagnetic resonance method was used to analyze in detail the existing forms of manganese ions in various antimony orefields in Qinglong Dachang, Guizhou Province. Combining with a large number of chemical analysis data, the distribution rules of manganese ions in orefields, It is pointed out that in the process of diagenesis and mineralization in Dachang orefield, manganese does not fully transfer and enrichment like antimony, and its geochemical behavior is “inert”, and the content of manganese in all kinds of minerals and rocks is very low , There is no manganese carrier minerals formed. At the same time, it further discusses that the study of manganese ions has the dual meaning of genesis and prospecting in solving some problems of metal deposits.